Features of the glacial history of the Transantarctic Mountains inferred from cosmogenic 26 Al, 10 Be and 21 Ne concentrations in bedrock surfaces

Abstract This paper describes measurements of concentrations of cosmogenic 26 Al, 10 Be and 21 Ne in quartz from bedrock surfaces in the Transantarctic Mountains where stratigraphic and geomorphic evidence shows that the surfaces were covered by ice in the past, but were not glacially eroded during...

Full description

Bibliographic Details
Published in:Antarctic Science
Main Authors: Balco, Greg, Stone, John O.H., Sliwinski, Maciej G., Todd, Claire
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2014
Subjects:
Online Access:http://dx.doi.org/10.1017/s0954102014000261
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102014000261